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Updated: Jun 10, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

鉄同位体制約は,アルカインとパレオプロテロゾーイク時代の海洋の酸化還元状態に影響した

Olivier J Rouxel1, Andrey Bekker, Katrina J Edwards

  • 1Marine Chemistry and Geochemistry Department, Geomicrobiology Group, Woods Hole Oceanographic Institution, Mail Stop 8, Woods Hole, MA 02543, USA. orouxel@whoi.edu

Science (New York, N.Y.)
|February 19, 2005
PubMed
まとめ

海洋の酸化還元状態は,大気中の酸素が上昇したことで,23億年前に変化した. 鉄同位体データは,海洋の鉄循環のシフトを明らかにし,層状の海洋における硫化鉄の降水量の増加を示しています.

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